FREE BOOKS

Author's List




PREV.   NEXT  
|<   45   46   47   48   49   50   51   52   53   54   55   56   57   58   59   60   61   62   63   64   65   66   67   68   69  
70   71   72   73   74   75   76   77   78   79   80   81   82   83   84   85   86   87   88   89   90   91   92   93   94   >>   >|  
ysicists have tried to calculate the age of the sun from the rate of its dissipation of heat, and have assigned, at the most, a hundred million years to our solar system; but the recent discovery of a source of heat in the disintegration of such metals as radium has made their calculations useless. Geologists have endeavoured, from observation of the action of geological agencies to-day, to estimate how long it will have taken them to form the stratified crust of the earth; but even the best estimates vary between twenty-five and a hundred million years, and we have reason to think that the intensity of these geological agencies may have varied in different ages. Chemists have calculated how long it would take the ocean, which was originally fresh water, to take up from the rocks and rivers the salt which it contains to-day; Professor Joly has on this ground assigned a hundred million years since the waters first descended upon the crust. We must be content to know that the best recent estimates, based on positive data, vary between fifty and a hundred million years for the story which we are now about to narrate. The earlier or astronomical period remains quite incalculable. Sir G. Darwin thinks that it was probably at least a thousand million years since the moon was separated from the earth. Whatever the period of time may be since some cosmic cataclysm scattered the material of our solar system in the form of a nebula, it is only a fraction of that larger and illimitable time which the evolution of the stars dimly suggests to the scientific imagination. THE GEOLOGICAL SERIES [The scale of years adopted--50,000,000 for the stratified rocks--is merely an intermediate between conflicting estimates.] ERA. PERIOD. RELATIVE LENGTH. Quaternary Holocene 500,000 years Pleistocene Tertiary Pliocene 5,500,000 years or Miocene Cenozoic Oligocene Eocene Secondary Cretaceous 7,200,000 years or Jurassic 3,600,000 " Mesozoic Triassic 2,500,000 " Primary Permian 2,800,000 years or Carboniferous 6,200,000 " Palaeozoic Devonian 8,000,000 " Silurian
PREV.   NEXT  
|<   45   46   47   48   49   50   51   52   53   54   55   56   57   58   59   60   61   62   63   64   65   66   67   68   69  
70   71   72   73   74   75   76   77   78   79   80   81   82   83   84   85   86   87   88   89   90   91   92   93   94   >>   >|  



Top keywords:

million

 

hundred

 
estimates
 

agencies

 
stratified
 

period

 

geological

 

recent

 

system

 

assigned


nebula

 

material

 

scattered

 

cataclysm

 

Carboniferous

 

fraction

 

Permian

 

suggests

 

evolution

 

larger


illimitable

 

cosmic

 

Darwin

 

Devonian

 
thinks
 
Silurian
 

Whatever

 

separated

 

Palaeozoic

 

thousand


scientific

 

Cenozoic

 

LENGTH

 

Quaternary

 
Cretaceous
 
RELATIVE
 

Secondary

 

PERIOD

 

Triassic

 
Mesozoic

Jurassic
 

Tertiary

 
incalculable
 
Holocene
 
conflicting
 
Miocene
 

Primary

 

SERIES

 

GEOLOGICAL

 
imagination